mantle convection

基本解釋

• 地函對(duì)流，[地物] 地幔對(duì)流；[地物] 地幔對(duì)流

英漢例句

雙語(yǔ)例句

• In mantle convection models, the mantle viscosity is generally assumed constant or dependent on depth.
  粘度為常數(shù)或僅隨深度變化是地幔對(duì)流模型中常用的假設(shè)。
• The ratio of poloidal to toroidal component of mantle convection determined the proportion of seismic energy released in the thrust, normal, or strike-slip earthquakes.
  地幔對(duì)流的垂直運(yùn)動(dòng)與水平運(yùn)動(dòng)分量的比率，決定了逆沖、引張與走滑型強(qiáng)震的能量釋放份額。
• A constant viscosity mantle convection model is developed into a variable viscosity model assumed a latitude-dependent viscosity with small fluctuations on the basis of a constant background value.
  建立了一維粘度擾動(dòng)下的變粘度模型。 通過(guò)假定粘度為常粘度背景下存在僅隨緯度變化的小橫向擾動(dòng)，將常粘度模型發(fā)展為變粘度地幔對(duì)流模型。

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詞組短語(yǔ)

短語(yǔ)

• Mantle wedge convection 地幔楔對(duì)流
• whole mantle wide convection 全地幔對(duì)流
• mantle convection circle 地幔對(duì)流環(huán)
• mantle convection theory 地套對(duì)流說(shuō)
• mantle 's convection 地幔對(duì)流

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專業(yè)釋義

地球科學(xué)

• 地幔對(duì)流

  In another hand, mantle convection process may directly influence the surface deformation movement of the region.
  另一方面，地幔對(duì)流對(duì)巖石層底部的拖曳作用將直接影響該區(qū)域巖石層形變運(yùn)動(dòng)。

• 地函對(duì)流